Assessment of North Sinai Shoreline Morphodynamics Using Geospatial Tools and DSAS Technique

This study employs a digital shoreline analysis system (DSAS) to identify and evaluate historical changes in the coastline along the North Sinai coast of Egypt. Using multi-temporal satellite images, change detection is explored along coastline over 27 years (1989–2016). The annualized uncertainty o...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Masria, Ali, Nassar, Karim, Eltarabily, Mohamed Galal
Formato: Capítulo de libro
Lenguaje:inglés
Publicado: IntechOpen 2022
Materias:
Acceso en línea:https://www.intechopen.com/chapters/81021
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
_version_ 1879164770963161088
author Masria, Ali
Nassar, Karim
Eltarabily, Mohamed Galal
author_browse Eltarabily, Mohamed Galal
Masria, Ali
Nassar, Karim
author_facet Masria, Ali
Nassar, Karim
Eltarabily, Mohamed Galal
author_sort Masria, Ali
building IntechOpen
collection Acceso abierto
description This study employs a digital shoreline analysis system (DSAS) to identify and evaluate historical changes in the coastline along the North Sinai coast of Egypt. Using multi-temporal satellite images, change detection is explored along coastline over 27 years (1989–2016). The annualized uncertainty of shoreline changes was calculated. Erosion and accretion patterns were automatically quantified via four statistical parameters in the DSAS model namely net shoreline movement (NSM), rate of −8.17 m year−1 was recorded at the west seaside of El-Tinah plain throughout the 27 years. This recession of the shoreline is attributed to the joint effect of the stormy climate of the western seaside and the sediments transport from the Nile Delta. shoreline has progressed west of El-Bardawil inlet towards El-Arish harbor, where wave-induced littoral transport is ceased by the construction of jetties. The shoreline at the downdrift side of the jetties to the east has adversely retreated where the subsequent beaches are reverted at rates of −4.5 and −2.9 m year−1. Lastly, the EPR model was utilized for quantifying shoreline changes in the near future of years 2025, 2035, and 2050.
doi_str_mv 10.5772/intechopen.103031
first_indexed 2026-10-15T21:39:37Z
format Book Chapter
fullrecord <oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><identifier>intech-81021</identifier><datestamp>2022-03-30</datestamp> <dc:title>Assessment of North Sinai Shoreline Morphodynamics Using Geospatial Tools and DSAS Technique</dc:title> <dc:creator>Ali Masria</dc:creator> <dc:creator>Karim Nassar</dc:creator> <dc:creator>Mohamed Galal Eltarabily</dc:creator> <dc:subject>Physical Sciences, Engineering and Technology</dc:subject> <dc:description>This study employs a digital shoreline analysis system (DSAS) to identify and evaluate historical changes in the coastline along the North Sinai coast of Egypt. Using multi-temporal satellite images, change detection is explored along coastline over 27 years (1989–2016). The annualized uncertainty of shoreline changes was calculated. Erosion and accretion patterns were automatically quantified via four statistical parameters in the DSAS model namely net shoreline movement (NSM), rate of −8.17 m year−1 was recorded at the west seaside of El-Tinah plain throughout the 27 years. This recession of the shoreline is attributed to the joint effect of the stormy climate of the western seaside and the sediments transport from the Nile Delta. shoreline has progressed west of El-Bardawil inlet towards El-Arish harbor, where wave-induced littoral transport is ceased by the construction of jetties. The shoreline at the downdrift side of the jetties to the east has adversely retreated where the subsequent beaches are reverted at rates of −4.5 and −2.9 m year−1. Lastly, the EPR model was utilized for quantifying shoreline changes in the near future of years 2025, 2035, and 2050.</dc:description> <dc:publisher>IntechOpen</dc:publisher> <dc:date>2022-03-30</dc:date> <dc:type>Chapter, Part Of Book</dc:type> <dc:identifier>https://www.intechopen.com/chapters/81021</dc:identifier> <dc:identifier>doi:10.5772/intechopen.103031</dc:identifier> <dc:language>en</dc:language> <dc:relation>ISBN:978-1-80355-741-0</dc:relation> <dc:rights>https://creativecommons.org/licenses/by/3.0/</dc:rights> <dc:source>https://www.intechopen.com/books/11134 ; Geographic Information Systems and Applications in Coastal Studies</dc:source> </oai_dc:dc>
id intech-81021
institution IntechOpen
isbn 978-1-80355-741-0
language English
last_indexed 2026-10-15T21:39:37Z
publishDate 2022
publishDateRange 2022
publishDateSort 2022
publisher IntechOpen
publisherStr IntechOpen
record_format oai_dc
spelling intech-810212022-03-30 Assessment of North Sinai Shoreline Morphodynamics Using Geospatial Tools and DSAS Technique Ali Masria Karim Nassar Mohamed Galal Eltarabily Physical Sciences, Engineering and Technology This study employs a digital shoreline analysis system (DSAS) to identify and evaluate historical changes in the coastline along the North Sinai coast of Egypt. Using multi-temporal satellite images, change detection is explored along coastline over 27 years (1989–2016). The annualized uncertainty of shoreline changes was calculated. Erosion and accretion patterns were automatically quantified via four statistical parameters in the DSAS model namely net shoreline movement (NSM), rate of −8.17 m year−1 was recorded at the west seaside of El-Tinah plain throughout the 27 years. This recession of the shoreline is attributed to the joint effect of the stormy climate of the western seaside and the sediments transport from the Nile Delta. shoreline has progressed west of El-Bardawil inlet towards El-Arish harbor, where wave-induced littoral transport is ceased by the construction of jetties. The shoreline at the downdrift side of the jetties to the east has adversely retreated where the subsequent beaches are reverted at rates of −4.5 and −2.9 m year−1. Lastly, the EPR model was utilized for quantifying shoreline changes in the near future of years 2025, 2035, and 2050. IntechOpen 2022-03-30 Chapter, Part Of Book https://www.intechopen.com/chapters/81021 doi:10.5772/intechopen.103031 en ISBN:978-1-80355-741-0 https://creativecommons.org/licenses/by/3.0/ https://www.intechopen.com/books/11134 ; Geographic Information Systems and Applications in Coastal Studies
spellingShingle Physical Sciences, Engineering and Technology
Masria, Ali
Nassar, Karim
Eltarabily, Mohamed Galal
Assessment of North Sinai Shoreline Morphodynamics Using Geospatial Tools and DSAS Technique
title Assessment of North Sinai Shoreline Morphodynamics Using Geospatial Tools and DSAS Technique
title_full Assessment of North Sinai Shoreline Morphodynamics Using Geospatial Tools and DSAS Technique
title_fullStr Assessment of North Sinai Shoreline Morphodynamics Using Geospatial Tools and DSAS Technique
title_full_unstemmed Assessment of North Sinai Shoreline Morphodynamics Using Geospatial Tools and DSAS Technique
title_short Assessment of North Sinai Shoreline Morphodynamics Using Geospatial Tools and DSAS Technique
title_sort assessment of north sinai shoreline morphodynamics using geospatial tools and dsas technique
topic Physical Sciences, Engineering and Technology
url https://www.intechopen.com/chapters/81021
work_keys_str_mv AT masriaali assessmentofnorthsinaishorelinemorphodynamicsusinggeospatialtoolsanddsastechnique
AT nassarkarim assessmentofnorthsinaishorelinemorphodynamicsusinggeospatialtoolsanddsastechnique
AT eltarabilymohamedgalal assessmentofnorthsinaishorelinemorphodynamicsusinggeospatialtoolsanddsastechnique